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Evidence for a major unconformity in Middle Triassic strata (Doig, Halfway and lowermost Charlie Lake formations) of the Grande Prairie area (Map-sheet 83 M; townships 70 to 80, ranges 1W6 to 13W6), west-central Alberta
Author(s) -
J Dixon
Publication year - 2004
Language(s) - English
Resource type - Reports
DOI - 10.4095/214886
Subject(s) - unconformity , geology , archaeology , geomorphology , paleontology , geography , sedimentary rock

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